• Aucun résultat trouvé

BD Entropy and Bernis-Friedman Entropy

N/A
N/A
Protected

Academic year: 2021

Partager "BD Entropy and Bernis-Friedman Entropy"

Copied!
8
0
0

Texte intégral

(1)

HAL Id: hal-01911965

https://hal.archives-ouvertes.fr/hal-01911965v2

Preprint submitted on 7 Nov 2018

HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci- entific research documents, whether they are pub- lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.

BD Entropy and Bernis-Friedman Entropy

Didier Bresch, Mathieu Colin, Khawla Msheik, Pascal Noble, Xi Song

To cite this version:

Didier Bresch, Mathieu Colin, Khawla Msheik, Pascal Noble, Xi Song. BD Entropy and Bernis-

Friedman Entropy. 2018. �hal-01911965v2�

(2)

BD Entropy and Bernis-Friedman Entropy

Didier Bresch a,1 , Mathieu Colin b,2 , Khawla Msheik a,1 , Pascal Noble c,3 , Xi Song

a

LAMA UMR5127 CNRS, Universit´ e Grenoble Alpes, Universit´ e Savoie Mont-Blanc, 73376 Le Bourget du Lac, France

b

Equipe INRIA CARDAMOM , IMB Equipes EDP, 351 cours de la lib´ eration, 33405 Talence, France

c

IMT, INSA Toulouse, 135 avenue de Rangueil, 31077 Toulouse Cedex 9, France

Received *****; accepted after revision +++++

Presented by

Abstract

In this note, we propose in the full generality a link between the BD entropy introduced by D. Bresch and B. Desjardins for the viscous shallow-water equations and the Bernis-Friedman (called BF) dissipative entropy introduced to study the lubrications equations. Different dissipative entropies are obtained playing with the drag terms on the viscous shallow water equations. It helps for instance to prove global existence of nonnegative weak solutions for the lubrication equations starting from the global existence of nonnegative weak solutions for appropriate viscous shallow-water equations.

R´ esum´ e

BD entropie et entropie de Bernis-Friedman. Dans cette note, on propose un lien g´en´eral entre la BD entropie introduite par D. Bresch et B. Desjardins pour les ´equations de Saint-Venant visqueuses et l’entropie dissipative de Bernis-Friedman (not´ee BF) introduite pour ´etudier les ´equations de lubrifications. Diff´erentes entropies dissipatives sont obtenues suivant le choix des termes de train´ee sur Saint-Venant visqueux. Ce lien entre ces deux outils math´ematiques aide par exemple ` a prouver l’existence de solutions faibles positives pour les

´equations de lubrification en partant de l’existence de solutions faibles positives pour des ´equations de Saint-Venant visqueuses bien choisies.

Email addresses: Didier.Bresch@univ-smb.fr (Didier Bresch), Mathieu.Colin@math.u-bordeaux.fr (Mathieu Colin), khawla.msheik@univ-smb.fr (Khawla Msheik), pascal.noble@math.univ-toulouse.fr (Pascal Noble),

xi.song@hotmail.com (Xi Song).

1 . Research of D.B. and K.M. was partially supported by the ANR project ANR-16-CE06-0011-02 FRAISE and ANR- 17-CE08-0030 ViSCAP. D.B. want to thank G. Kitavtsev for his comments and suggestions.

2 . Research of M.C. was partially supported by the ANR project ANR-17-CE08-0030 ViSCAP

3 . Research of P.N. was partially supported by the ANR project BoND ANR-13-BS01-0009-01 .

(3)

Version fran¸ caise abr´ eg´ ee

Dans cette note, on propose un lien g´en´eral entre la BD entropie introduite par D. Bresch et B. Des- jardins pour les ´equations de Saint-Venant visqueuses (voir [2] et [3]) et l’entropie dissipative de Bernis- Friedman (que l’on notera BF) introduite (voir [6]) pour ´etudier les ´equations de lubrifications. Diff´erentes entropies dissipatives sont obtenues suivant le choix des termes de train´ee sur Saint-Venant visqueux g´en´eralisant ainsi quelques travaux importants comme [12], [9]. Ce lien entre les deux outils importants que sont la BD entropie et la BF entropie permet par exemple de construire des solutions faibles du mod`ele de lubrification ` a partir de solutions faibles du mod`ele de Saint-Venant. Il permet ´egalement d’obtenir certains r´esultats sur les ´equations de Saint-Venant en s’inspirant des r´esultats ´etablis sur les

´equations de lubrification qui ont ´et´e beaucoup plus ´etudi´ees historiquement. Le syst`eme de lubrification s’´ecrit par exemple

∂ t h + ∂ x ( 1 αW e

h nx 3 h − 1

αF r 2 h m−1 ∂ x h) = 0 et le mod`ele de Saint–Venant associ´e

 

 

∂ t h ε + ∂ x (h ε u ¯ ε ) = 0, ε ∂ t (h ε u ¯ ε ) + ∂ x (h ε ¯ u 2 ε )

! + 1

F r 2 h β ε ∂ x (h ε ) = ε 4 R e

∂ x (h ε ∂ x u ¯ ε )

! + 1

W e

h ε ∂ x 3 h ε − α h 2 ε u ε

h n ε , (1) o` u β + n = m : voir par exemple [4], [5] ou [2]. Nous discuterons des deux outils importants que sont la BF entropie et l’entropie dissipative dˆ ue ` a Bernis-Friedman (BF). Nous expliquerons l’int´erˆet qu’il y a de mettre en exergue une telle relation. On peut par exemple ´etudier ces syst`emes et montrer l’existence globale de solutions faibles du mod`ele de lubrification en partant de solutions faibles positives du mod`ele de Saint-Venant associ´e. On peut ´egalement consid´erer des syst`emes avec des termes non-locaux en s’inspirant de r´esultats r´ecents, voir par exemple [11], [8].

1. Introduction: Lubrication systems and viscous shallow-water equations with drag terms.

In this section, we present the formal link between two key tools respectively for lubrication system by Bernis-Friedman and for shallow-water equations by Bresch-Desjardins. We first start by presenting the two quantities and their link on a simple example and then we explain how to get relations in a more general case. Our calculations remain at this stage only formal. We assume solutions are regular enough.

1.1. A lubrication system: energy estimate and Bernis-Friedman (BF) dissipative entropy

In a one dimensional periodic domain Ω, consider the following thin-film equation, also known as lubrication equation

∂ t h + ∂ x ( 1 αW e

F (h)∂ x 3 h − 1

αF r 2 F (h)∂ x h) = 0. (2) We couple this equation with the initial condition

h(x, 0) = h 0 (x) in Ω System (2) can be rewritten equivalently as a gradient flow system

∂ t h + ∂ x (hu) = 0, hu = 1

αW e

F (h)∂ x 3 h − 1

αF r 2 F (h)∂ x h. (3)

2

(4)

The corresponding energy is given, for all t ∈ (0, T ), by Z t

0

Z

αh 2 u 2

F (h) dx dt + 1 2 Z

h(x, t) 2

F r 2 + (∂ x h(x, t)) 2 W e

dx = 1 2

Z

h 0 (x) 2

F r 2 + (∂ x h 0 (x)) 2 W e

dx. (4) In their paper [6], Bernis and Friedman proved the existence of a weak solution for a higher order nonlinear degenerate parabolic equations and suggested a new entropy inequality- referred to by BF entropy- which provides additional estimates serving for increasing the regularity of the weak solution obtained. As for our problem, we adapt the same methodology to obtain the BF entropy of the general lubrication model stated above. Indeed, define the functionals

g ε (s) = − Z A

s

1

F (r) + ε dr, G ε (s) = − Z A

s

g ε (r) dr,

with A being an integer such that A ≥ max |h(x, t)|. According to Bernis and Friedman, we multiply (2) by G

0 (h), where G 0 = lim

ε→0 G ε , we get the BF dissipative entropy equality Z

G 0 (h(x, T )) dx + Z T

0

Z

(∂ x 2 h) 2 αW e

+ (∂ x h) 2

αF r 2 dx dt = Z

G 0 (h 0 (x)) dx. (5)

1.2. A viscous shallow–water system: energy estimate and BD entropy

In a periodic domain Ω, let us consider the viscous Shallow Water system with surface tensions and a drag term:

 

 

∂ t h ε + ∂ x (h ε u ¯ ε ) = 0, ε ∂ t (h ε u ¯ ε ) + ∂ x (h ε u ¯ 2 ε )

!

+ h ε ∂ x (h ε )

F r 2 = ε 4 R e

∂ x (h ε ∂ x u ¯ ε )

! + 1

W e

h ε ∂ 3 x h ε − α h 2 ε u ε

F(h ε ) . (6) The initial conditions are given by

h ε | t=0 = h ε 0 , (h ε u ¯ ε )| t=0 = m ε 0 .

α is a positive constant, R e , W e and F r are respectively the adimentional Reynold, Weber and Froude numbers. Note that the terms in the right-hand side of the momentum equation represent respectively the viscous term, the capillary term and the drag term. The energy equation corresponding to (6) is given, for all t ∈ (0, T ) by

Z

ε h ε (x, t)¯ u 2 ε (x, t)

2 + h ε (x, t) 2

2F r 2 + (∂ x h ε (x, t) 2 2W e

dx +

Z t 0

Z

4ε R e

h ε (∂ x u ¯ ε ) 2 + α h 2 ε u 2 ε

F (h ε ) dx dt (7)

= 1 2 Z

ε (m ε 0 ) 2 h ε 0

+ (h ε 0 ) 2

F r 2 + (∂ x h ε 0 ) 2 W e

dx.

As introduced in [2], the BD entropy equality is obtained by deriving the mass equation in space and multiplying by 4ε/R e then summing with the momentum equation, and multiplying the sum by the artificial velocity

v ε = ¯ u ε + 4 R e

∂ x (log(h ε )).

The BD entropy for the general system is given, for all t ∈ (0, T ), by

(5)

ε 2

Z

h ε (x, t)v ε (x, t) 2 dx + 1 2

Z

h ε (x, t) 2

F r 2 + (∂ x h ε (x, t)) 2 W e

dx

#

+ α Z t

0

Z

h 2 ε u ¯ 2 ε

F (h ε ) dx dt + 4 R e

" Z

Z t 0

(∂ x h ε ) 2

F r 2 + (∂ xx h ε ) 2 W e

dx dt + α Z t

0

Z

h ε u ¯ ε

F(h ε ) ∂ x h ε dx dt

| {z }

X

#

= ε 2

Z

Z

h ε 0 (x)v ε (x, 0) 2 dx + 1 2 Z

h ε 0 (x) 2

F r 2 + (∂ x h ε 0 (x)) 2 W e

dx.

(8)

As for the term X, it can be rewritten as X =

Z

h ε u ¯ ε

∂ x h ε

F (h ε ) dx = Z

h ε u ¯ ε

d dx

Z h

ε

A

1 F (y) dy

dx

= Z

−∂ x (h ε u ¯ ε ) Z h

ε

A

1 F (y) dy

dx

= Z

∂ t h ε

Z h

ε

A

1 F (y) dy

dx.

1.3. The link between the BD entropy and the BF dissipative entropy In view of the term X and G 0 , we noticed the following

G

0 (h ε ) = g 0 (h ε ) = − Z A

h

ε

1 F (r) dr =

Z h

ε

A

1s F (r) dr.

Hence

X = Z

∂ t h ε G

0 (h ε ) dx = d dt

Z

G 0 (h ε ) dx.

Thus, coupled with (7), the BD entropy reads:

ε 2

Z

h ε (x, t)v ε (x, t) 2 dx − ε 2 Z

h ε (x, t)¯ u ε (x, t) 2 dx − 4ε R e

Z t 0

Z

h ε (∂ x u ¯ ε ) 2 + 4

R e

" Z

Z t 0

(∂ x h ε ) 2

F r 2 + (∂ xx h ε ) 2 W e

dx dt + α Z

G 0 (h ε (x, t)) dx

#

= − 1 2

Z

ε (m ε 0 ) 2 h ε 0 + ε

2 Z

h ε 0 (x)v ε (x, 0) 2 dx + 4α R e

Z

G 0 (h ε 0 ) dx.

(9)

If we assume now that the couple (h ε , u ¯ ε ), solution of (6), converges in a proper sense to (h, u), then we find that the above BD entropy equality degenerates to the following inequality, which coincides with the dissipative BF-entropy of (2)

Z

Z t 0

(∂ x h) 2

αF r 2 + (∂ xx h) 2 αW e

dx dt + Z

G 0 (h(x, t)) dx = Z

G 0 (h 0 (x)) dx. (10) Of course these computations are formal and have been written with equalities but they help to under- stand that the BF entropy may be obtained from the BD entropy. This provides a way to construct nonnegative solutions of lubrication equation from nonnegative solutions of the shallow water equation with appropriate drag terms. Let us present below a general computation with different surface tension and pressure term showing the relation between the BD entropy and the BF dissipative entropy.

4

(6)

2. A general link between the BD entropy and the BF dissipative entropy

In this part, we will consider the following fourth order lubrication approximation that has been studied in several papers, see for instance [4], [5]:

∂ t h + ∂ x ( 1 αW e

F(h)∂ x 3 h − 1

αF r 2 D(h)∂ x h) = 0. (11) In [4] for instance, the authors considered the above lubrication model with the following choice of F and D: F (h) = h n and D(h) = h m−1 . Indeed, the lubrication equation becomes:

∂ t h + ∂ x ( 1 αW e

h n ∂ x 3 h − 1

αF r 2 h m

1 ∂ x h) = 0. (12) In fact, they proved the existence of a global in time nonnegative weak solution starting from nonnegative datum for all n > 0, and 1 < m < 2. In particular, The most critical case is the most significantly physical one when n = 3 (moving contact line in a thin film). In this case, a distributional solution is proven to exist, where it becomes a strong positive solution in the infinite time limit. In this sequel, we will consider the choices of F and D stated above. Then, the BF entropy corresponding to the latter system is given by

Z

G 0 (h(x, T )) dx + Z T

0

Z

(∂ 2 x h) 2 W e + 1

F r 2 h m−n−1 (∂ x h) 2 dx dt = Z

G 0 (h 0 (x)) dx. (13) Consider herein the following Shallow water system with drag term corresponding to a weight F (h) = h n

 

 

∂ t h ε + ∂ x (h ε u ¯ ε ) = 0, ε ∂ t (h ε u ¯ ε ) + ∂ x (h ε u ¯ 2 ε )

! + 1

F r 2 h β ε ∂ x (h ε ) = ε 4 R e

∂ x (h ε ∂ x u ¯ ε )

! + 1

W e

h ε ∂ x 3 h ε − α h 2 ε u ε

h n ε

, (14)

where β + n ∈ (1, 2). The energy and BD entropy of system (14) are given respectively by 1

2 Z

εh ε (x, T )¯ u 2 ε (x, T ) + 1 F r 2

h ε (x, T ) β+1

β(β + 1) + (∂ x h ε (x, T )) 2 W e

dx +

Z T 0

Z

4ε R e

h ε (∂ x u ¯ ε ) 2 + α h 2 ε u 2 ε

h n ε dx dt

= 1 2

Z

ε (m ε 0 ) 2 h ε 0 + 1

F r 2

(h ε 0 ) β+1

β(β + 1) + (∂ x h ε 0 ) 2 W e

dx.

and ε 2

Z

h ε (x, T )v ε (x, T ) 2 − h ε (x, T )¯ u ε (x, t) 2 dx + 4 Re

Z T 0

Z

1

F r 2 h β ε

1 (∂ x h ε ) 2 dx + 1 W e

(∂ xx h ε ) 2 dx dt + 4

Re Z

G 0 (h ε (x, T )) dx − 4ε Re

Z T 0

Z

h ε (∂ x u ¯ ε ) 2 dx dt

= ε 2

Z

h ε 0 v ε (x, 0) 2 − m ε 0 h ε 0

dx + 4 Re

Z

G 0 (h ε 0 (x)) dx.

Under the assumption of the convergence results, and choosing m = β + n ∈ (1, 2), we get that the BD

entropy degenerates as well to the BF dissipative entropy of system (12) given by (13). Remark that the

link between the BD entropy and the BF entropy may also be done in higher dimensions, see [10] for BF

entropy and [3] for BD entropy. This could help to perform the analysis in the bi-dimensional setting.

(7)

3. Mathematical results obtained using the link between BD and BF entropies

In this part, we aim at proving the existence of a global in time weak solution for the lubrication model by passing to the limit in the viscous shallow water model with two different choices of the drag term, corresponding to two weights: F(h) = h 2 which results in a linear drag term, and F(h) = h 2 + h 3 which yields a nonlinear drag term. The latter weight has been used by A.L.Bertozzi in the physical and mathematical justification of the lubrication model [4]. The main theorem states:

Theorem 3.1 Given a sequence (h ε , u ¯ ε ) ε a global weak solution of (6), where h ε 0 ≥ 0, then there exists a subsequence of (h ε , u ¯ ε ) such that (h ε , u ¯ ε ) converges to (h,u) a global weak solution of the lubrication system (2) satisfying h ≥ 0, and the initial condition h| t=0 = h 0 , where h 0 is the weak limit of h ε 0 in H 1 (Ω).

The proof of the limit of the viscous shallow water model into a lubrication model is summarized in the following steps:

(i) Assuming that (6) possesses a weak solution (h ε , u ¯ ε ), bring first the physical energy and BD-entropy estimates to get uniform bounds of the system’s unknowns and thus get weak convergence up to a subsequence of these terms. Such solution has been constructed by D. Bresch and B. Desjardins in [2]. See also [13] for more general interesting studies related to 1D compressible Navier-Stokes.

(ii) Use compactness theory to obtain strong convergence (mainly for h ε ).

(iii) Pass the limit in the weak formulation of (6) to obtain that the solution is a weak solution of the lubrication theory.

It is important to remark that some studies have already analyzed the limit process from shallow-water to lubrication systems but with special pressure terms, see the nice papers [14], [12] and recently [9].

See also the recent paper [7] where dissipative systems may be obtained from shallow-water type system through a quadratic change of time and no need of a priori drag terms. Note that in [12] and [9], BD and BF entropies are interconnected for F (h) = h. In [11], we can find a result concerning the global existence of non-negative solutions for electrified thin films. Such systems contain nonlocal terms. As an example consider the following system

∂ t h + ∂ x (h 3 ∂ x (∂ x 2 h − I(h))) = 0 in Ω = (0, 1) where I(h) is a non-local elliptic operator of order 1 given by

I(h) = Z

(h(y) − h(x))ν(x, y) dy where for all x, y ∈ Ω

ν(x, y) = π 2

1

1 − cos(π(x − y)) + 1

1 − cos(π(x + y)) .

The system is supplemented by the following boundary and initial conditions

∂ x h = h 3 ∂ x (∂ x 2 h − I(h)) = 0 on ∂Ω, h| t=0 = h 0 for x ∈ Ω.

It is interesting to see that in order to construct a solution to this lubrication equation, one can consider the following shallow-water model

 

 

∂ t h ε + ∂ x (h ε u ¯ ε ) = 0, ε ∂ t (h ε u ¯ ε ) + ∂ x (h ε u ¯ 2 ε )

!

+ h ε ∂ x I(h ε ) = ε∂ x (h ε ∂ x u ¯ ε ) + h ε ∂ x 3 h ε − α u ε

h ε

, (15)

6

(8)

with appropriate boundary conditions. Then using the energy estimate and the BD entropy, we can pass to the limit and get the global existence of non-negative solutions of the system studied in [11]. Note that compressible Navier-Stokes system with constant viscosities and non-local term has been studied recently in [8] together with the long-time behavior of its solutions. The details will be given in the forthcoming paper [1].

References

[1] D. Bresch, M. Colin, K. Msheik, P. Noble, X. Song. Lubrication/shallow-water system: BD and Bernis-Friedman entropies. Forthcoming paper (2018).

[2] D. Bresch, B. Desjardins. Existence of global weak solutions for a 2D viscous shallow water equations and convergence to the quasi-geostrophic model Com. Math. Phys, 238 (1-2), 211–223, (2003).

[3] D. Bresch, B. Desjardins. Quelques mod` eles diffusifs capillaires de type Korteweg, C. R. M´ ecanique, 332, 881–886, (2004).

[4] A.L. Bertozzi, M. Pugh. The lubrication approximation for thin viscous films: the moving contact line with a ”porous media”” cut-off of van der Waals interactions. Nonlinearity, 7(6), 1535–1564, (1994).

[5] A.L. Bertozzi, M.C. Pugh. Long-wave instabilities and saturation in thin film equations. Com. Pure Appl. Math., 51(6), 625–661, (1998).

[6] F. Bernis, A. Friedman. Higher order nonlinear degenerate parabolic equations. J. Diff. Eqs, 83(1), 179–206, (1990).

[7] Y. Brenier, X. Duan. From conservative to dissipative systems through quadratic change of time, with application to the curve-shrotening flow. Arch Rational Mech. Analysis, 227, 545–565, (2018).

[8] J.A. Carillo, A. Wr´ oblewska-Kami´ nska, Z. Zatorska. On long-time asymptotic for viscous hydrodynamic models of collective behaviour with damping and nonlocal interactions. Math. Models Methods Appl. Sci. To appear in (2018).

[9] M. A Fontelos, G. Kitavtsev, R. M. Taranets. Asymptotic decay and non-rupture of viscous sheets. Z. Angew. Math.

Phys. 69–79, (2018).

[10] G. Gr¨ un, On Bernis interpolation inequalities in multiple space dimensions, Z. Anal. Anwend. 20 (2001) 987998, (2001).

[11] C. Imbert, A. Mellet. Electrified thin films: Global existence of non-negative solutions. Annales de lIHP, analyse non- lin´ eaire Vol 29, No 11, 413-433, (2012).

[12] G. Kitavtsev, P. Lauren¸cot, B. Niethammer. Weak solutions to lubrication equations in the presence of strong slippage.

Methods Appl. of Analysis, 18, 2, 183–202, (2011).

[13] H.L. Li, J. Li, Z.P. Xin. Vanishing of vacuum states and blow-up phenomena of the compressible Navier-Stokes equations.

Comm. Math. Phys, 281–301, (2008).

[14] A. M¨ unch, B.A. Wagner, T.P. Witelski. Lubrication models with small to large slip lengths. J. Engineering Math., 53,

3–4, 359–383, (2005).

Références

Documents relatifs

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des

In this work, we are interested in the solution of the planar Riemann problem for an enriched two dimensional shallow water type model where the horizontal..

In this note, we show a global weak existence result for a two dimensionnal Compressible Primitive Equations for atmosphere dynamics modeling.. Keywords: Atmosphere modelling, a

The damping coefficient for decay with time is used to determine the minimum critical wind speed for the initiation of wave growth in shallow water by the instability mechanism of

For the blow-up result in the slow diffusion case, Ishida and Yokota [13] proved that every radially symmetric energy solution with large negative initial energy blows up in

Global weak entropy solutions to Navier–Stokes Doi–Saintillan–Shelley model In this section, we prove the following theorem..

Quantum computation is mostly seen as a static process: we are given an algo- rithm A that must be decomposed in elementary computational steps which have to be unitary operators

Abstract: From the study of a functional equation relating the Gibbs measures at two different tempratures we prove that the specific entropy of the Gibbs measure of